地理科学

地理科学 ›› 2011, Vol. 31 ›› Issue (12): 1430-1436.doi: 10.13249/j.cnki.sgs.2011.012.1430

• 论文 • 上一篇    下一篇

1956～2000年中国地表水资源状况:变化特征、成因及影响

张强1,2, 孙鹏1,2, 陈喜3, 陈晓宏1,2   

  1. 1. 中山大学水资源与环境系, 广东广州510275;
    2. 中山大学华南地区水循环与水安全广东省普通高校重点实验室, 广东广州510275;
    3. 河海大学水文水资源与水利工程科学国家重点实验室, 江苏南京210098
  • 收稿日期:2011-01-17 修回日期:2011-04-02 出版日期:1997-12-20 发布日期:1997-12-20
  • 基金资助:
    国家自然科学基金项目(41071020;50839005);广东省科技厅对外合作项目(2010B050800001;2010B050300010);中山大学理工科青年教师重点培育计划项目(2009-37000-1132381)资助

Water Resources in China from 1956 to 2000:Changing Properties,Causes and Implications

ZHANG Qiang1,2, SUN Peng1,2, CHEN Xi3, CHEN Xiao-hong1,2   

  1. 1. Department of Water Resources and Environment, Sun Yat-sen University, Guangzhou, Guangdong 510275, China;
    2. Guangdong University Key Laboratory of Water Cycle and Security in South China, Sun Yat-sen University, Guangzhou Guangdong 510275, China;
    3. State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing Jiangsu 210098, China
  • Received:2011-01-17 Revised:2011-04-02 Online:1997-12-20 Published:1997-12-20

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被引次数

47

摘要： 系统搜集了中国590个雨量站和383个水文站1956~2000年长序列月降水量与月径流量资料,及1978~2000年全国各省、自治区的旱涝受灾与成灾面积、灌区面积、已建水库库容等数据资料,全面分析了地表径流时空演变特征以及农业旱涝灾害的时空分布特征,并分析了其原因及可能影响,研究结果表明,中国北方降水减少,其中山东和黄河中游地区的降水量减小最显著。另外,冬季降水增加明显,而春秋季降水减少明显,极易导致春秋旱灾;北方地区降水减少是造成地表径流量减小的主要原因,农业灌溉进一步加剧地表径流量减小,南方径流量的增加主要是由降水量增加引起的;降水时空分布不均匀造成水资源分布不均,进而造成大部分地区农业受旱涝灾害面积呈增加趋势,其中旱灾受灾面积远大于水灾的受灾面积;农村水利基础设施(灌区、水库等)能提高地区的抗旱能力,但是对洪涝灾害的影响没有旱灾那么明显。节水灌溉技术的推广应用是北方地区在水资源短缺的前提下保证农业生产稳定的重要措施。

Abstract: Changes of water resources in China are the key scientific problem in terms of sustainable development of agriculture and social security.Based on long-term hydro-meteorological dataset,i.e.daily precipitation data from 590 rainfall gauging stations and monthly streamflow from 383 hydrological stations covering 1956~2000 over China,water resources in China are thoroughly evaluated.Impacts of human activities,the agricultural irrigation in this study,on water resources are also analyzed.Besides,the data concerning the flood-and drought-affected and the flood-and drought-destroyed agricultural fields are also collected and analyzed with Mann-kendall and Kriging interpolationaim to discuss the implications of precipitation changes and streamflow variations on agriculture in China.This study produced important and novel conclusions: ① decreasing precipitation is found in north China,particularly in the Shandong and the middle Yellow River.The south China is dominated by increasing precipitation.In addition,decreasing precipitation is prevailing in spring and autumn which may easily cause droughts in spring and autumn.The winter is characterized by increasing precipitation.② Decreasing surface streamflow is the result of decreasing precipitation.The agricultural irrigation further intensifies the decreasing magnitude of streamflow in north China.This result further corroborates the tremendous human influences on water resources in north China.③ Uneven distribution of precipitation leads to uneven spatial patterns of water resources over China.Agricultural activities in China are mostly under the risk of drought and flood hazards.Drought hazards may play the dominant role in the loss of agricultural production.④ the irrigation facilities are urgently calling for great concerns.Besides,water-saving agriculture is also the major effective way to mitigate water shortage due to climate changes and intensifying human interference with water resource system of China.

中图分类号: 

  • F512.2